中文摘要：

在从南船座介绍的 situ 观察，与卫星相结合的漂流检索了 SST，雨率被用来通过 2012 年 8 月 29 日从 20 调查上面的海洋回答到台风 Bolaven。在台风 Bolaven 的经过以后，加深混合的层深度(MLD ) ，并且冷却混合的层温度(MLT ) 被观察。在混合的层咸度(MLS ) 的变化显示出因为在混合的层的导致台风的咸度变化被降水，蒸发，狂暴的混合和 thermocline 水的 upwelling 影响，增加并且减少的一个相等的数字。加深 MLD 并且冷却 MLT 显示了重要向右偏爱，而 MLS 被添到台风轨道的左边并且在另外的方面上增加了。铱漂流观察的集中的温度和咸度侧面使在台风的经过以后在上面的海洋看反应过程可能。冷却在近表面并且温暖在表面下被在暴风雨的开发阶段期间定位到气旋的磁道的左边的二铱漂流观察，在远处，最大值的半径相对台风中心弯屈。在混合的层的底和 thermocline 的顶的水咸度增加是那些二漂流观察的最明显的变化。在轨道并且在台风中心附近的右边上当台风被加强时，从海表面的重要冷却到 200 的深度

英文摘要：

In situ observations from Argo profiling floats combined with satellite retrieved SST and rain rate are used to investigate an upper ocean response to Typhoon Bolaven from 20 through 29 August 2012. After the passage of Typhoon Bolaven, the deepening of mixed layer depth（MLD）, and the cooling of mixed layer temperature（MLT） were observed. The changes in mixed layer salinity（MLS） showed an equivalent number of increasing and decreasing because the typhoon-induced salinity changes in the mixed layer were influenced by precipitation, evaporation, turbulent mixing and upwelling of thermocline water. The deepening of the MLD and the cooling of the MLT indicated a significant rightward bias, whereas the MLS was freshened to the left side of the typhoon track and increased on the other side. Intensive temperature and salinity profiles observed by Iridium floats make it possible to view response processes in the upper ocean after the passage of a typhoon. The cooling in the near-surface and the warming in the subsurface were observed by two Iridium floats located to the left side of the cyclonic track during the development stage of the storm, beyond the radius of maximum winds relative to the typhoon center. Water salinity increases at the base of the mixed layer and the top of the thermocline were the most obvious change observed by those two floats. On the right side of the track and near the typhoon center when the typhoon was intensified, the significant cooling from sea surface to a depth of 200×10^4 Pa, with the exception of the water at the top of the thermocline, was observed by the other Iridium float. Owing to the enhanced upwelling near the typhoon center, the water salinity in the near-surface increased noticeably. The heat pumping from the mixed layer into the thermocline induced by downwelling and the upwelling induced by the positive wind stress curl are the main causes for the different temperature and salinity variations on the different sides of the track. It seems that more time is requir